Observations of Outward-propagating and Mirroring of the Same Energetic Electrons by Wind
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Explore the source record for details and available documents.
Explore the source record for details and available documents.
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Electron flux and its relationship to auroral absorption of radio waves
Injun 1 satellite observations to show the relationship between auroral absorption of radio waves and electron fluxes
Energy spectrum change of group of electrons being convected downwind in magnetosheath and behind Earth bow shock
Diffusion effects on energy spectrum of electron group analyzed during downwind convection in bow shock transition region of earth
OGO outer zone observational data on electron intensities of earth geomagnetic field
Spatial distribution data for electron flux behind earth bow shock during dusk and dawn
Variations of electron flux density observations by Explorer 12 and 14
Time profiles of trapped Van Allen electrons in auroral zones
Substorm-associated acceleration effects on electron increases in post-midnight sector of outer radiation belt
Active region MacMath no. 8905 proding 16 distinct electron events associated with solar flares during passage across solar disk
Distinct Kev electron events as observed by satellites near the earth are, in general, associated with solar flares which are accompained by the emission of both metric and hectometric type 3 radio bursts. The positions of these flares are mainly on the western hemisphere of the sun. These results show that Kev electrons propagate under the control of the magnetic field in the interplanetary space and that, while propagating through this space, these electrons excite type 3 radio bursts from metric to hectometric wave frequencies. Emission characteristics of hectometric type 3 bursts are briefly considered in relation to the positions of associated flares.
Quantitative study of the intrusion of natural electrons into the inner radiation zone during and after the geomagnetic storm of Sept. 2, 1966. It is shown that the transport is consistent with a radial-diffusion mechanism in which the first two invariants are conserved. Except for the three-day period of the storm main phase when data were missing, the radial-diffusion coefficient is found to have a value which could be produced by a variation of a large-scale electric field across the magnetosphere having an amplitude of 0.28 mV/m and a period of 1600 sec. Electric fields having approximately these characteristics have been inferred from previous observations of the motion of whistler ducts within the plasmapause. If fields of this amplitude and period exist throughout the magnetosphere, the radial diffusion of all geomagnetically trapped particles except the high-energy inner-zone protons is strongly influenced by electric-field variations. A comprehensive review of previously reported radial-diffusion coefficients shows reasonable agreement for L less than about 3.0, but serious discrepancies among reported values exist for determinations made in the outer zone. These discrepancies cannot be explained by the simple theory of radial diffusion due to variation of large-scale electric or magnetic fields.